5:eaau8932. In addition to TPST, global warming, interannual, and interdecadal variability, such as WNPSH, ENSO, PDO, and AMO, can also influence the summer rainfall in this area. At 200 hPa, another wave train propagated downstream along the upper–level westerly jet stream and strong anticyclones appear over the South China Sea (Figures 8B–F). Sci., 26 November 2020
Sci. Appl. Bollasina Massimo, A., and Gabriele, M. (2018). Similarly, as the mountain is set farther into Tibet than Everest, the rainy season brings more rains that can make traveling around the kora route very dangerous. All of them are statistically significant at the 95% confidence level. The variable selection procedure is shown in Table 2. In this study, the spatiotemporal distributions of monthly and annual temperature minima (T min) and maxima (T max), extreme T min and T max, the highest (lowest) T min (T max), frost day (FD), icing day (ID), summer day (SD) and tropical night (TR) at 112 stations and over the ten large river basins on the Tibetan Plateau and its surroundings (TPS) during 1963–2015 are examined. The Qinghai-Tibet Plateau Meteorology. While most trends are local in nature, there are general basinwide patterns. Everest Base Camp has a typical plateau monsoon climate, with both wet and dry seasons. Si and Ding (2013) suggested that the relationship between the Tibetan Plateau winter snow and the SCSSMP changed in 1999. Once the monsoon season is over, there is very little chance of rain in Shigatse throughout the winter months, and from December to the end of February the land is cold and dry, with strong biting winds. When to come is entirely up to you, and the best time for any trip to Tibet depends largely on what you want to see and where you want to go. Understanding of effects of soil temperature and soil moisture on soil respiration (Rs) under future warming is critical to reduce uncertainty in predictions of feedbacks to atmospheric CO2 concentrations from grassland soil carbon. However, the nighttime drop in temperature is equally as large, with temperatures dropping to as low as minus 7 degrees in December and January. Hollow rhombuses indicate significant differences above the 90% confidence level based on the Student's t–test. Dyn.
Let. (2008). Sci. The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. Rev. Summer temperatures of Shigatse range from 18-22 degrees during the day, but drop to an average of between 5 and 7 degrees at night. Change. Standardized partial regression coefficients between Tibetan Plateau temperature at station and OLR in East Asia: (a) for the period from 1980 to 1994 and (b) for the period from 1998 to 2016. The weather in spring and autumn is ideal for trekking, with drier weather and less rain, clear skies and relatively warm temperatures. To take you to the best of Tibet in the best time, we offer various kinds of Tibet group tours with frequent departure dated during the whole year. 52, 3997–4009. (2013). The Qinghai-Tibet Plateau (QTP) holds massive freshwater resources and is one of the most active regions in the world with respect to the hydrological cycle. Conversely, it is the winter months from December and January that get the most sunshine, with between 24 and 26 sunny days a month. (2009). Time to make the most of the weather and clear skies before the cold sets in. Clim. We add the variables of PDO, ENSO, and AMO by one after another. The solid lines are time series of Tibetan Plateau summer temperature during 1980–2016 for different datasets. Finally, uncertainties remain because our understanding of the linkage between the TPST and SCSSMP is based on statistical analyses. At the same time, a strong anticyclone is also found over the Northern China and it also means the negative correlation between them. 24, 793-807. doi: 10.1007/s00382-004-0488-8, Duan, A. M., and Wu, G. X. In each step, the variable with the smallest p values which <0.1 is added to the model. Res. Wu and Liu (2000) furtherly developed the thermal adaptation theory (a prescribed deep/shallow convective-type heating). Thermal adaptation, overshooting, dispersion, and subtropical high. 9, 112-130. doi: 10.1007/BF02656935, Ding, Y. H., Sun, Y., Wang, Z., Zhu, Y., and Song, Y. For the download websites and resolutions of all above datasets, please see Table 1 for detail. To reduce the error, all reanalysis datasets are interpolated to the resolution of 1.25° latitude × 1.25° longitude. P < 0.01 indicates a significant difference above the 99% confidence level. J. 59, 5–31. 35, L14702. 30, 5205–5220. Clim. A study of the role of the Tibetan Plateau's thermal forcing in modulating rainband and moisture transport in eastern China (in Chinese). In the following study, we will use the ECHAM 6 numerical model to further verify our findings and understand the mechanism of the change relationship between TPST–SCSSMP. Famous for the peach blossoms that bloom on the thousands of trees across the prefecture every April, Nyingchi is one of the lowest places on the Tibetan plateau, with an average elevation of around 3,000 meters. 26, 7622–7634. Received: 15 July 2020; Accepted: 26 October 2020; Published: 26 November 2020. Quantitative analysis of surface warming amplification over the Tibetan Plateau after the late 1990s using surface energy balance equation. A New Grid for the IFS. Thermal controls on the Asian summer monsoon. Red dashed lines represent wave-like structures. 39, 1169-1181. doi: 10.1007/s00382-012-1334-z, Wu, G. X., Liu, Y. M., He, B., Bao, Q., Duan, A. M., and Jin, F. F. (2012a). The purple boxed areas represent the South China Sea. The values of the trends differ slightly among the data sets, but both methods detected consistent increasing trends (P < 0.01). Intact cores with roots taken from a full factorial, 5-year alpine … In other words, during 1998–2016, the area is more prone to precipitation when the convection conditions are suitable. 98, 3011. doi: 10.1029/2017EO083011, Strong, G. S., Proctor, B., Wang, M., Soulis, E. D., Smith, C. D., Seglenieks, F., et al. The lowest temperature recorded was in the county of Karasjok, which is located on the Finnmark Plateau. Beijing: Science Press. A plateau scale soil moisture and soil temperature observatory is established on the Tibetan Plateau for quantifying uncertainties in coarse resolution satellite and model products of soil moisture and soil temperature. , Shanghai and Chengdu the East Asian summer monsoon pressure, pt 500 hPa, V the structure!, 1980–1994 and 1998–2016, respectively in these reanalysis datasets you book early us... Strong anticyclone is also used rainfall in this study, we should be cautious when using predictor with interdecadal in. 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